The fault-slip burst has the features of high frequency, considerable damage and complex
mechanisms, because mining activities break the balance of energy in the system of the fault …

As coal mining depth and structural complexity increase, the failure severity of mining-
induced fault activation leading to rock bursts escalates. Fault fracture zones, consisting of …

Viscous salt layers can introduce significant structural complexity to the basins in which they
are deposited. Along basin margins, salt typically flows seaward due to regional tilting of the …

Despite salt being regarded as an extremely efficient, low‐permeability hydraulic seal, an
increasing number of cross‐evaporite fluid escape features have been documented in salt …

Episodic venting from deep overpressured layers has rarely been documented in
sedimentary basins, so the pressure evolution leading to these cyclical phenomena is poorly …

The Messinian salt layer in the eastern Mediterranean region plays a key role in the
Pliocene-Quaternary deformation and formation of the tectonic structures in the Levant …

Salt basins often exhibit a shelf/slope region of extension and a deeper domain of
contraction. The up‐slope normal faults in such salt tectonics systems are often associated …

Fluid venting phenomena are prevalent in sedimentary basins globally. Offshore, these
localized fluid-expulsion events are archived in the geologic record by the resulting …

Fluid venting poses clear risks to various industrial applications including carbon dioxide
sequestration. To assess these risks, a detailed understanding of the conditions for fluid …

Predicting the distribution of sedimentary facies during the early stages of deformation of salt-
detached continental margins is key to constraining the location and stratigraphic …